Palaeoenvironments of the last Neanderthals in SW Europe (MIS 3): Cova del Coll Verdaguer (Barcelona, NE of Iberian Peninsula)

Marine isotope stage 3 (MIS 3) was characterised by marked oscillations of extreme cold episodes with very short warm events during the stadial, and several regional differences have been recorded in the ice cores and marine deposits. The aim of this study is to reconstruct this period by evaluating...

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Detalhes bibliográficos
Autor principal: Daura, Joan (author)
Outros Autores: Sanz, Montserrat (author), Allué, E. (author), Vaquero, M. (author), López-García, J.M. (author), Sánchez-Marco, A. (author), Domènech, R. (author), Martinell, J. (author), Carrión, J.S. (author), Ortiz, J.E. (author), Torres, T. (author), Arnold, L.J. (author), Benson, A. (author), Hoffmann, D.L. (author), Skinner, A.R. (author), Julià, R. (author)
Formato: article
Idioma:eng
Publicado em: 2018
Assuntos:
Late Pleistocene
MIS 3
Cova del Coll Verdaguer
Palaeoenvironment
Iberian Peninsula
Texto completo:http://hdl.handle.net/10451/31370
País:Portugal
Oai:oai:repositorio.ul.pt:10451/31370

Texto Completo

http://hdl.handle.net/10451/31370

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